Hostname: page-component-76d6cb85b7-2r2wp Total loading time: 0 Render date: 2026-07-16T10:55:19.062Z Has data issue: false hasContentIssue false

Stimulation for geothermal wells in the Netherlands

Published online by Cambridge University Press:  05 February 2020

C.J. (Hans) de Pater*
Affiliation:
Fenix Consulting Delft BV, Poortweg 6A, 2612 PADelft, the Netherlands
Josef R. Shaoul
Affiliation:
Fenix Consulting Delft BV, Poortweg 6A, 2612 PADelft, the Netherlands
*
Author for correspondence: Hans de Pater, Email: hans.depater@fenixdelft.com

Abstract

Hydraulic fracturing is a long-established method of stimulating a well to improve the inflow or outflow potential. Hydraulic fracturing is the most successful stimulation method used by the oil and gas industry, and is also used for water injection and production wells around the world, even for drinking-water wells. Hydraulic fracturing creates a crack in the earth that is then filled with a highly conductive material (proppant). This fracture has a large inflow area compared to an unstimulated wellbore and provides a high-permeability path for the fluid to flow in or out of the reservoir.

Hydraulic fracturing has a long history of being used in hot dry rock (HDR) geothermal applications since the 1980s (Murphy & Fehler, 1986). In those often very tight reservoirs, the aim is to create fracture networks that generate the reservoir flow capacity. In high-permeability formations, fracturing can potentially double the productivity of a well. In low-permeability formations, well performance can be increased by a factor of 5–10 in most cases.

In this paper, we focus on two different scenarios of geothermal stimulation. The first is for permeable, porous formations where the heat exchange happens through the perfect contact between the fluid and the porous reservoir. Stimulation may then be necessary to create a small fracture if the pressure drop near the well is too large due to insufficient reservoir permeability. The other scenario is a formation at great depth, where the formation permeability is so extremely small that very long propped fractures would be needed to obtain sufficient flow or even where the porous system does not provide sufficient heat exchange but the heat exchange has to be facilitated by an artificial or stimulated fracture network: a so-called Enhanced Geothermal System.

For porous, permeable formations we will present examples of fracture treatments that can increase the flow rate so that the economics of the project is improved. In some formations, stimulation is then a contingency in case of poorer than expected reservoir quality. A worst-case well with a large skin value of 20 can perform with stimulation like a base-case unstimulated well. In other formations, stimulation will be integral to well design in order to optimise the project performance. For those cases the Coefficient of Performance can be improved from 7 to 25 with the aid of stimulation.

In Ultra-Deep Geothermal (UDG) recovery, the targets are reservoirs below 4000 m, because industrial heat demand requires a minimum temperature of 120°C up to 250°C. For an economic business case, the rate over a period of 15 to 25 years should be from 150 to 450 m3 h−1, depending on the boundary conditions.

Shallower reservoirs in the Netherlands often show very high permeability, but at great depth the target layers could have very low permeability (Veldkamp et al., 2018). Several stimulation methods can be used, of which hydraulic fracture stimulation with water (proppantless) is the primary candidate. Other stimulation methods are propped fracturing in sandstone, acid fracturing in carbonates and thermal stimulation.

For a geological play that is attractive for UDG in the Netherlands, the most likely stimulation method is with water fracturing, because propped fracturing would require a huge amount of proppant that is very costly. Based on analogues and conceptual designs, the expected flow rate is estimated under selected boundary conditions.

Information

Type
Original Article
Creative Commons
Creative Common License - CCCreative Common License - BY
This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited.
Copyright
© The Author(s) 2020
Figure 0

Figure 1. Idealised hydraulic fracture geometry for a vertical wellbore.

Figure 1

Figure 2. Inflow geometry for wellbore and hydraulic fracture.

Figure 2

Figure 3. Skin bypass fracture in high-permeability formation.

Figure 3

Figure 4. Frac pack completion string.

Figure 4

Figure 5. Horizontal well with multiple longitudinal fractures.

Figure 5

Table 1. Reservoir parameters for den Haag producer analogue well

Figure 6

Table 2. Reservoir parameters for den Haag injector analogue well

Figure 7

Table 3. Fluid properties for den Haag analogue

Figure 8

Table 4. Rock modulus estimates

Figure 9

Figure 6. Simulated fracture dimensions and conductivity for P50 producer well.

Figure 10

Table 5. Treatment design for den Haag P50 producer well fracture stimulation

Figure 11

Table 6. Flow rate and drawdown for the unstimulated cases with skin and the stimulated case

Figure 12

Figure 7. Productivity index (PI) of production well for matrix flow and a fractured well, normalised on the PI of a zero skin well in the P50 case.

Figure 13

Table 7. Parameters used in the calculation of pump energy and COP (Robertson, 1988)

Figure 14

Table 8. Well injection pressure (in m water) and drawdown for different cases and skin values. The fracture case is assumed to bypass any skin

Figure 15

Table 9. Computed pump energy and resulting COP, computed with the simulation results in Table 8

Figure 16

Figure 8. Conceptual model of planar propped fracture system.

Figure 17

Figure 9. Conceptual model of fracture network.

Figure 18

Figure 10. Simulation model that uses a quarter symmetry block around one fracture. The fluid pressure in the fracture causes fracture opening which induces conductivity of the fracture. Heat transfer in the fracture and surrounding rock is simulated with convection conduction including fluid infiltration from the fracture. The water is injected at 40°C with constant rate, and production is at the same rate. The production temperature is computed as a function of time.

Figure 19

Figure 11. Temperature along the fracture for different injection times.

Figure 20

Figure 12. Pressure along the fracture, which changes somewhat over time due to changing fluid viscosity with temperature.

Figure 21

Figure 13. Production temperature vs time.